Lamonte trevallis explained

Lamonte trevallis is an ichnospecies from the late Ediacaran sediments of the Yangtze Gorges of Southern China. [1] It represented fairly large traces that indicate burrowing behaviour.[2] [3] It had Millimetre-sized traces preserved differently than other Ichnofossils from that time period.[1] Surface-dwelling trackways, vertical burrows and horizontal tunnels are a common characteristic of the trace fossil.

See also

Notes and References

  1. Beyond the stony veil: Reconstructing the Earth's earliest large animal traces via computed tomography X-ray imaging . 10.1016/j.precamres.2017.05.010 . 2017 . Meyer . Mike . Polys . Nick . Yaqoob . Humza . Hinnov . Linda . Xiao . Shuhai . Precambrian Research . 298 . 341–350 . 2017PreR..298..341M . 10919/81948 . free .
  2. 10.1016/j.palaeo.2013.12.026. Interactions between Ediacaran animals and microbial mats: Insights from Lamonte trevallis, a new trace fossil from the Dengying Formation of South China. Palaeogeography, Palaeoclimatology, Palaeoecology. 396. 62–74. 2014. Meyer . M. . Xiao . S. . Gill . B. C. . Schiffbauer . J. D. . Chen . Z. . Zhou . C. . Yuan . X. . 2014PPP...396...62M.
  3. 10.1016/j.precamres.2020.105768. Petrographic evidence for Ediacaran microbial mat-targeted behaviors from the Great Basin, United States. Precambrian Research. 345. 105768. 2020. O'Neil . G. O. . Tackett . L. S. . Meyer . M. . 2020PreR..34505768O. 218916532.

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